2017
DOI: 10.1016/j.clay.2017.03.037
|View full text |Cite
|
Sign up to set email alerts
|

Relationship between the thermal behaviour of the clays and their mineralogical and chemical composition: Example of Ipoh, Kuala Rompin and Mersing (Malaysia)

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
13
0
24

Year Published

2017
2017
2023
2023

Publication Types

Select...
8
1
1

Relationship

0
10

Authors

Journals

citations
Cited by 33 publications
(37 citation statements)
references
References 17 publications
0
13
0
24
Order By: Relevance
“…The SiO 2 /Al 2 O 3 ratio also provides information on the amount of quartz that may be present in the starting clays [ 36 ]. A high SiO 2 /Al 2 O 3 ratio indicates a greater amount of quartz in the raw material.…”
Section: Resultsmentioning
confidence: 99%
“…The SiO 2 /Al 2 O 3 ratio also provides information on the amount of quartz that may be present in the starting clays [ 36 ]. A high SiO 2 /Al 2 O 3 ratio indicates a greater amount of quartz in the raw material.…”
Section: Resultsmentioning
confidence: 99%
“…The origin of clay minerals affected its chemical properties and its resulting derived materials [37][38][39][40]. The resulting bricks varied in chemical and textural compositions from one place to another, depending on their geological origin and the presence of organic and inorganic impurities [41][42][43]. This study was carried out to test the hypothesis that the waste bricks obtained from different areas, using different clays, could affect their physiochemical properties and if the resulting waste materials would be effective in the removal of BB-41 in various conditions.…”
Section: Introductionmentioning
confidence: 99%
“…Additionally, the dimensional changes presented about 1% linear shrinkage. This observed effect is well known and is associated with the removal of absorbed water and water contained within the pore network [47][48][49]. Moreover, the sample size expansion recorded on the dilatometric curve ( Figure 17) in the temperature ranged from 300 • C to 600 • C can be attributed to a dehydroxylation process and the polymorphic α-β transition of an unreacted quartz phase or glass transition in the geopolymer matrix [50].…”
Section: Thermal Analysis Of the Geopolymer Synthesized At Optimum Comentioning
confidence: 72%